Lava flows are gravity currents of partially molten rock that cool as they flow, in some cases
melting the surface over which they flow but in all cases gradually solidifying until they come …

▪ Abstract Pahoehoe lava flows are common in every basaltic province, and their submarine
variants, pillow lavas and sheet flows, cover the bulk of the Earth. Pahoehoe flows are …

Large igneous provinces (LIPs) are sites of the most frequently recurring, largest volume
basaltic and silicic eruptions in Earth history. These large-volume (> 1000km3 dense rock …

We present studies on the physical volcanology of the∼ 15 Ma Roza Member of the
Wanapum Formation in the Columbia River Basalt Group. The Roza Member represents a …

Measurement of effusion rate is a primary objective for studies that model lava flow and
magma system dynamics, as well as for monitoring efforts during on-going eruptions …

We present a kinematic, self-adaptive, numerical model to describe the down-flow thermal
and rheological evolution of channel-contained lava. As our control volume of lava …

Iceland is one of the most active and productive terrestrial volcanic regions, with eruption
frequency of≥ 20 events per century and magma output rates of≥ 5 km3 per century …

Silicic volcanic rocks are associated with most, if not all, continental flood basalt provinces
and volcanic rifted margins, where they can form substantial parts of the eruptive …

ABSTRACT The middle Miocene Columbia River Basalt Group is the youngest and smallest
continental flood basalt province on Earth, covering over 210,000 km2 of mainly Oregon …

The present study is probably the first of its kind in the Deccan Volcanic Province (DVP) that
deals in detail with the morphology and emplacement of the Deccan Trap flows, and …